{"refrec":{"BRefID":233838,"RR":"<b>Reimer, J.J.; Vargas, R.; Smith, S.V.; Lara-Lara, J.R.; Gaxiola-Castro, G.; Hernandez-Ayon, J.M.; Castro, A.; Escoto-Rodriguez, M.; Martínez-Osuna, J.</b> (2013). Air-sea CO<sub>2</sub> fluxes in the near-shore and intertidal zones influenced by the California Current. <i>J. Geophys. Res. Oceans 118(10)</i>: 4795–4810. <a href=\"http://dx.doi.org/10.1002/jgrc.20319\" target=\"_blank\">http://dx.doi.org/10.1002/jgrc.20319</a>","BEntID":225523,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>J. Geophys. Res. Oceans 118(10)</i>: 4795–4810. <a href=\"http://dx.doi.org/10.1002/jgrc.20319\" target=\"_blank\">http://dx.doi.org/10.1002/jgrc.20319</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Reimer, J.J.; Vargas, R.; Smith, S.V.; Lara-Lara, J.R.; Gaxiola-Castro, G.; Hernandez-Ayon, J.M.; Castro, A.; Escoto-Rodriguez, M.; Martínez-Osuna, J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Reimer, J.J. <i>et al.</i>","Englishabstract":"[1]</span> The study of air-sea CO<sub>2</sub> fluxes (<em>F</em>CO<sub>2</sub>) in the coastal region is needed to better understand the processes that influence the direction and magnitude of <em>F</em>CO<sub>2</sub> and to constrain the global carbon budget. We implemented a 1 year (January through December 2009) paired study to measure <em>F</em>CO<sub>2</sub> in the intertidal zone (the coastline to 1.6 km offshore) and the near-shore (~3 km offshore) off the north-western coast of Baja California (Mexico); a region influenced by year-round upwelling. <em>F</em>CO<sub>2</sub> was determined in the intertidal zone via eddy covariance; while in the near-shore using mooring buoy sensors then calculated with the bulk method. The near-shore region was a weak annual net source of CO<sub>2</sub> to the atmosphere (0.043 mol CO<sub>2</sub> m<sup>-2</sup> y<sup>-1</sup>); where 91% of the outgassed <em>F</em>CO<sub>2</sub> was contributed during the upwelling season. Sea surface temperature (SST) and ?<em>p</em>CO<sub>2</sub> (from upwelling) showed the strongest relationship with <em>F</em>CO<sub>2</sub> in the near-shore, suggesting the importance of meso-scale processes (upwelling). <em>F</em>CO<sub>2</sub> in the intertidal zone were up to four orders of magnitude higher than <em>F</em>CO<sub>2</sub> in the near-shore. Wind speed showed the strongest relationship with <em>F</em>CO<sub>2</sub> in the intertidal zone, suggesting the relevance of micro-scale processes. Results show that there are substantial spatial and temporal differences in <em>F</em>CO<sub>2</sub> between the near-shore and intertidal zone; likely a result of heterogeneity. We suggest that detailed spatial and temporal measurements are needed across the coastal oceans and continental margins to better understand the mechanisms which control <em>F</em>CO<sub>2</sub>, as well as reduce uncertainties and constrain regional and global ocean carbon balances.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Air-sea CO<sub>2</sub> fluxes in the near-shore and intertidal zones influenced by the California Current","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-15 01:32:37.924177","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Air-sea CO2 flux","OtherDescriptors":null,"Notes":null,"AnaPub":2013,"MonPub":null,"DateUpdate":"2014-02-28","DateCreate":"2014-02-25","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000327380100004","VABBcode":null,"OpenAcc":0,"DOI":"10.1002/jgrc.20319"},"refs":null,"anarec":{"AnaID":233838,"PubliDate":2013,"Pagination":"4795–4810","XtraPublOfAnaID":null,"ISBN":null,"Volume":"Oceans 118","Issue":"10","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":90908,"SerRR":"Journal of Geophysical Research. 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